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Nitrogen cycling in low oxygen regions: how do autonomous, sustained observations factor into the debate on the role of classical denitrification versus anammox Ken Johnson MBARI
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Where does NO3- go?
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Free energy change (ΔG° kJ/4 e-)
Oxic Respiration: O2 + ½C2H3O2- HCO3- + ½ H+ Denitrification: 4/5NO3- + ½C2H3O2- + 3/10H+ 2/5N2 + HCO3- + 2/5H2O DNRA: ½NO3- + ½C2H3O2- + 1/2H+ + 1/2H2O 1/2NH4+ + HCO3- Anammox: NH4+ + NO2- N2 + 2H2O
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Mean Conc Input/ Loss Process Residence Time PO43- 2 µmol/L 2x1010 mol/y River input (Paytan & McLaughlin 2009) 100,000 years NO3- 30 µmol/L 230 Tg/y x 14 g/mol Global denitrification (Devries et al 2012) 2,500 years Ocean volume 1.4x1021 Liters Residence time = time required to add (or remove) the amount now present in the ocean.
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Eastern Tropical North Pacific (ETNP)
6960, 7558 Arabian Sea 6381
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Rates measured with incubations using 15N labeled substrates.
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Arabian Sea Denitrification dominates Eastern Tropical South Pacific Anammox dominates
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Anammox rate Denitrification rate
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To get N*, we need PO43-, which we don’t measure!
(PO43-) = (PO43-)preformed + AOU * 1/150 (PO43-)preformed = x T x T x Longitude x Latitude
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N* at 200 m (Gruber and Sarmiento, 1997)
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Float 6960 ETNP
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Float 7558 ETNP
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Float 6381 Arabian Sea
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Arabian Sea
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Arabian Sea Denitrification dominates Eastern Tropical South Pacific Anammox dominates
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Anammox rate (mmol N/m2/d)
Anammox rate (mmol N/m2/d). Dashed line is region with high NO2- (Naqvi, 1991).
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Arabian Sea -5 µmol/L/ 45 days = 50 nmol N2/L/d -5 µmol/L/
45 days x 200 m = 22 mmol/m2/d
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Float 6960 ETNP
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5 µmol/L is a typical deficit in the N* minima
If they have a time scale of about 2 weeks 5 µmol/L /14 d = 14 nmol/L/h
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Anammox rate Denitrification rate
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Physics has a big influence on observations (Float 7558 ETNP, 220 to 240 m)
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Arabian Sea -5 µmol/L/ 45 days = 50 nmol N2/L/d -5 µmol/L/
45 days x 200 m = 22 mmol/m2/d
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The N-Cycle is highly perturbed
The N-Cycle is highly perturbed. Human production of fixed nitrogen (nitrate, ammonia, urea) now exceeds the natural rate on land. The Economist, May 26, 2011
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Norman Borlaug, father of the “Green Revolution” and 1970 Nobel Peace Prize winner -- “the application of low-cost nitrogen derived from synthetic ammonia, has become an indispensable component of modern agricultural production (nearly 80 million tonnes consumed annually). It is estimated that 40% of today’s 6 billion people are alive, thanks to the Haber-Bosch process of synthesizing ammonia” (Borlaug, 2000). The Borlaug “Hypothesis”: Higher agricultural yields are critical to preventing further deforestation – (but more generally high yields can limit NET environmental impact because less land is converted to agriculture, my interpretation).
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Distance from Coast (km) Number of Papers % Negative O2 Trend
0-30 41 70.7 30-100 19 68.4 100+ 40 77.5 Published time series Distance from Coast (km) Number of Sites % Negative O2 Trend 0-30 424 64.2 30-100 632 57.6 100+ 2330 49.1 Analyze entire data set (all time series)
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